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首页> 外文期刊>Mapan: Journal of Metrology Society of India >Chemical Characterization of Cobalt Crust from Afanasy-Nikitin Seamount in the Eastern Indian Ocean by Inductively Coupled Plasma Time-of-Flight Mass Spectrometry
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Chemical Characterization of Cobalt Crust from Afanasy-Nikitin Seamount in the Eastern Indian Ocean by Inductively Coupled Plasma Time-of-Flight Mass Spectrometry

机译:电感耦合等离子体飞行时间质谱仪对印度洋东部阿凡纳西-尼基廷海山钴壳的化学表征

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Analytical methodology was developed for the chemical characterization of cobalt crust samples collected from the Afanasy-Nikitin seamount in Eastern Equatorial Indian Ocean by inductively coupled plasma time-of-flight mass spectrometry (ICP-TOF-MS). Concentrations of geochemically significant groups of different trace elements such as large-ion-lithophile elements (e.g., Rb, Cs), high field strength elements (e.g., Ta, Nb, Hf and Zr), rare earth elements in addition to a few major and minor elements were determined in these samples. Samples (~50 mg) were digested in closed digestion vessels for 48 h before the expulsion of Si and the residues were taken in 5 % nitric acid. ~(103)Rh was used as an internal standard. Matrix matching external calibrations were utilized in order to compensate for the spectroscopic and non-spectroscopic interferences. The detection limits obtained for various elements were in the range 1-0.01 ng/ml for majority of the elements analyzed. Accuracy for the determination of different elements is assessed by measuring them in a few cobalt crust samples, ferromanganese nodules and similar marine sediment reference materials. Also, there is a very good agreement between the data sets obtained by ICP-TOF-MS as well as the well established ICP-quadrupole MS on cobalt crust samples. The precisions obtained in this study are <5 % RSD for majority of the elements with comparable accuracy. The results are in agreement with certified and reference values wherever available for comparison. The geochemical characteristics of these rare marine sediments have been described.
机译:开发了用于通过电感耦合等离子体飞行时间质谱(ICP-TOF-MS)从赤道东印度洋Afanasy-Nikitin海山收集的钴结壳样品进行化学表征的分析方法。不同微量元素(例如大离子亲石元素(例如,Rb,Cs),高场强元素(例如,Ta,Nb,Hf和Zr),稀土元素等的地球化学重要组的浓度)在这些样品中测定了微量元素。在排出硅之前,将样品(〜50 mg)在密闭的消化容器中消化48 h,并将残留物溶于5%的硝酸中。 〜(103)Rh用作内标。利用矩阵匹配的外部校准来补偿光谱和非光谱干扰。对于所分析的大多数元素,各种元素的检出限在1-0.01 ng / ml的范围内。通过测量一些钴结壳样品,锰铁结核和类似的海洋沉积物参考材料中的各种元素,可以确定不同元素的准确性。而且,ICP-TOF-MS所获得的数据集与钴壳样品上建立完善的ICP-四极杆MS有着很好的一致性。对于大多数元素,在这项研究中获得的精度相对标准偏差<5%。只要有可比较的结果,结果均与认证值和参考值一致。已经描述了这些稀有海洋沉积物的地球化学特征。

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